Le quartzite à mica de la Haute-Côte-Nord : approche pétroarchéologique et technologique sur l'outillage lithique du site de Longue-Rive (DdEh-8), Haute Côte-Nord
|Advisor:||Chabot, Jacques; Woollett, James|
|Abstract:||Archaeological excavations at the DdEh-8 site carried out by the Ministère du Transport du Québec in 2013 as part of the Longue-Rive municipality highway bypass project in the Upper North Shore region produced an artifact collection associated with a Meadowood occupation (3000 to 2400 AA). More than 80% of the artifacts recovered are derived from the production of tools from a micaceous quartzite specific to this region. Lithologic variability of this regional micaceous quartzite remains poorly understood and its origin unknown. This thesis seeks to clarify the nature of this raw material which is ubiquitous in lithic assemblages from North Shore archaeological sites. We analyze the lithological variability of this material within the assemblage recovered at the DdEh-8 site and propose a more precise characterization based on thin-section petrography. This micaceous quartzite appears to be the result of mylonitization through shear zone deformation. Four main varieties are described and their use in tool production is documented using detailed typo-morphological and technological analyses. This thesis examines the production of lithic bifaces at DdEh-8 in depth; bifacial tools are a particularly significant part of the collection due to the systematic production of Meadowood-style “quaternary preforms” at the site. The classification of bifaces by stage of reduction was undertaken with a continuum approach correlating bifacial margin length with flake removal scar frequency. It appears that the reduction of bifaces at DdEh-8 is not strictly phased in clear technological steps although the objective of this reduction is indeed focused on the production of quaternary preforms. Mica quartzite is a highly favoured raw material in this bifacial industry for reasons that appear to us to be both practical and ideological; this material is both suitable and widely available in the region, while white quartzites appear to have been preferred in general elsewhere in the Meadowood Interaction Sphere|
|Document Type:||Mémoire de maîtrise|
|Open Access Date:||12 July 2021|
|Collection:||Thèses et mémoires|
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